中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Hydrologic processes of groundwater in a small monsoon-influenced mountainous watershed

文献类型:期刊论文

作者Yuan, Ruiqiang1; Wang, Shiqin2; Yang, Lihu3; Liu, Jianrong3; Wang, Peng4; Song, Xianfang3
刊名HYDROLOGY RESEARCH
出版日期2018-12-01
卷号49期号:6页码:2016-2029
关键词bedrock percolation groundwater recharge hydrologic processes mountain block recharge mountainous watershed North China Plain
ISSN号0029-1277
DOI10.2166/nh.2018.030
通讯作者Yuan, Ruiqiang(rqyuan@sxu.edu.cn)
英文摘要Mountain block recharge is the least well quantified owing to the lack of a thorough understanding of mountain block hydrological processes. Observations of spatio-temporal variations of groundwater were employed to clarify hydrologic processes in a semi-arid mountainous watershed of northern China. Results showed that the annual feeding rate of precipitation changed between 21% and 40%. However, infiltration of precipitation was mainly drained as interflow on slopes and recharged into the mountain valley as focused recharge. As a result, the mean correlation coefficient between precipitation and groundwater level was only 0.20 and seasonal variations were reduced. Mountain slope is essentially impermeable with no bedrock percolation under arid circumstances. Only a bedrock percolation event occurred after multiple closely-spaced heavy rains during the four-year observation, which induced a local rapid ascending of the water table and an enhanced lateral recharge from upgradient watersheds. The influence of the enhanced lateral recharge lasted three years, suggesting a huge groundwater catchment overcoming local watershed divides in mountain blocks. The average of the gradual recession of the water table was 5.1 mm/d with a maximum of 11.4 mm/d in the beginning stage. Both interflow and bedrock percolation are important. Our results highlight the changeability of hydrologic processes in mountain watersheds.
WOS关键词BLOCK RECHARGE ; STABLE-ISOTOPES ; FRONT ; BALANCE ; FLOW ; CATCHMENTS ; HILLSLOPE ; BASEFLOW ; MODEL ; STEEP
资助项目National Natural Science Foundation of China[41301033] ; Institute of Geographical Sciences and Natural Resources Research[2012ZD003] ; Water and Soil Conservation Station of Baoding
WOS研究方向Water Resources
语种英语
WOS记录号WOS:000452413800023
出版者IWA PUBLISHING
资助机构National Natural Science Foundation of China ; Institute of Geographical Sciences and Natural Resources Research ; Water and Soil Conservation Station of Baoding
源URL[http://ir.igsnrr.ac.cn/handle/311030/51373]  
专题中国科学院地理科学与资源研究所
通讯作者Yuan, Ruiqiang
作者单位1.Shanxi Univ, Coll Environm & Resources, Taiyuan 030006, Shanxi, Peoples R China
2.Chinese Acad Sci, Inst Genet & Dev Biol, Ctr Agr Resources Res, Shijiazhuang 050021, Hebei, Peoples R China
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
4.Jiangxi Normal Univ, Sch Geog & Environm, Nanchang 330022, Jiangxi, Peoples R China
推荐引用方式
GB/T 7714
Yuan, Ruiqiang,Wang, Shiqin,Yang, Lihu,et al. Hydrologic processes of groundwater in a small monsoon-influenced mountainous watershed[J]. HYDROLOGY RESEARCH,2018,49(6):2016-2029.
APA Yuan, Ruiqiang,Wang, Shiqin,Yang, Lihu,Liu, Jianrong,Wang, Peng,&Song, Xianfang.(2018).Hydrologic processes of groundwater in a small monsoon-influenced mountainous watershed.HYDROLOGY RESEARCH,49(6),2016-2029.
MLA Yuan, Ruiqiang,et al."Hydrologic processes of groundwater in a small monsoon-influenced mountainous watershed".HYDROLOGY RESEARCH 49.6(2018):2016-2029.

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来源:地理科学与资源研究所

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